Makatite is a very rare sodium silicate mineral typically found in saline lake deposits and alkaline igneous complexes. It usually forms soft, pearly, platy crystals that are extremely sensitive to environmental conditions, often dehydrating if removed from their native brine environment.
Is this makatite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch makatite with a known reference. Makatite sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to dull.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: acicular.
Often confused with
Makatite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside makatite
Minerals reported to co-occur with makatite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Si₄O₈(OH)₂·4H₂O
- Mohs hardness
- 3-4
- Density
- 1.97-2.07 g/cm³
- Streak
- White
- Luster
- Vitreous to dull
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Acicular
- Cleavage
- One, parallel to longitudinal axis, excellent
- Fluorescence
- Pale green under SW UV; yellow-white under LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In cores from drill holes in a lacustrine evaporite series (Lake Magadi, Kenya); leached from natrosilite in an alkalic pegmatite in a differentiated alkalic massif (Lovozero massif, Russia)
Where rockhounds find makatite
Classic worldwide localities
- Lake Magadi, Rift Valley, Kenya
- Mt. Alluaiv, Lovozero massif, Kola Peninsula, Russia
- Höwenegg quarry, Hegau, Baden-Württemberg, Germany
- Mont Saint-Hilaire and near Saint-Amable, Quebec, Canada
- Aris quarry, about 25 km south of Windhoek, Namibia
Field-hunting tip
Where it forms: In cores from drill holes in a lacustrine evaporite series (Lake Magadi, Kenya); leached from natrosilite in an alkalic pegmatite in a differentiated alkalic massif (Lovozero massif, Russia). If you start seeing trona, erionite, magadiite in float, you are in the right ground. Typical habit: acicular. Train your eye for that shape before scanning the outcrop.





